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Dinosaur Remains

Recent Finds and Research


Caulkicephalus trimicrodon - a new species of flying reptile from the Isle of Wight - 2005

New pterosaur from the Isle of Wight!
Around 125 million years ago, the carcase of a pterosaur was washed into the mud at the bottom of a river. It lay there undisturbed until a few years ago, when coastal erosion removed it from its rocky tomb. Parts of the skull and wing bones were found on the beach by several different local collectors. Other parts may have been washed away already.

Pterosaurs were winged reptiles that lived at the same time as dinosaurs. The earliest pterosaurs are found in Triassic rocks in Italy, around 235 million years old. They survived until the end of the Cretaceous Period, by which point many large forms existed, with wingspans of over 12 metres. The reason for their extinction 65 million years ago is a mystery, but it was the end for many other animal and plant groups on Earth.

The new pterosaur from Sandown Bay belongs to a family called the Ornithocheiridae (‘bird hand’). They are large pterosaurs with crested skulls, long pointed teeth, and wingspans of around 4-6 metres. Ornithocheirids have been found in Cretaceous rocks in many parts of the world, particularly the UK, Brazil and North Africa.

The Sandown pterosaur is different from any that have been previously discovered, so it has been given a new name: Caulkicephalus trimicrodon. The generic name is derived from ‘caulkhead’, the traditional local name for people who caulked ships in the Solent shipyards. The species trimicrodon refers to the three small teeth near the front of the jaw.

The bones, which include the braincase, upper jaw and wing bones, were found on Yaverland beach by G. Leng, T. Winch, D. Davies, M. New, M. Munt, and L. Steel. The new pterosaur is described in the latest issue of the scientific journal Cretaceous Research, by a scientific team including Dinosaur Isle Museum, University of Portsmouth and the Humboldt Museum in Berlin.

The full reference is:
Steel, L., Martill, D. M., Unwin, D. M. & Winch, J. D. (2005) A new pterodactyloid pterosaur from the Wessex Formation (Lower Cretaceous) of the Isle of Wight, England. Cretaceous Research (2005): 1-13.


Skull reconstruction

Skull reconstruction by Lorna Steel

Figure 1.  A reconstruction of the skull of Caulkicephalus trimicrodon by Lorna Steel.

The rostrum ('upper jaw')

Palatal view of rostrum

Figure 2.  Palatal view of the rostrum of C. trimicrodon

Rostrum - right lateral view

Figure 3.  Right lateral view of the rostrum

Drawing of the distal portion of the rostrum

Figure 4.  Drawing of the distal portion of the rostrum

The two images shown in Figures 3 and 4 show the right lateral view of the rostrum (or upper part of the jaw). The rostrum is in three parts as can be seen in the photograph (Figure 2). The sockets for the teeth show that there are two prominent forward facing teeth at the snout, with three larger teeth behind on each side. Just to the left of the fracture (Figure 4) are sockets for three small teeth on each side. It is this feature that gives the species its name (trimicrodon = three-small-teeth). From this point back the teeth are staggered in alternate positions as can be seen in the palatal views below and in Figure 2. The preserved part of the rostrum is 29cm in length.

Palatal view of rostrum (proximal)
Palatal view of rostrum (distal)

Figure 5.  Drawings of the palatal view of the rostrum.

Anterior view of the rostrum Figure 6.  Anterior view of the rostrum.

This view of the 'snout' shows the position of the forward facing tooth sockets (dental alveoli). The small black spot seen in one of the sockets is the tip of a replacement tooth.

Figure 7.  An unrelated pterosaur tooth shown for comparison.



Unrelated pterosaur tooth

 The braincase

Posterior view of braincase

Figure 8.  Posterior view of the partial braincase.

Associated with the rostrum was a partial braincase which is assumed to come from the same individual.  The image shows the back (posterior) view and the base of the skull crest.

 

 

 

 

 


School find - 7th July 2005
Crocodile toothOn the 7th July 2005 this large fossil crocodile tooth was found by James, a Year 5 pupil from Birdham C of E Primary School, Chichester. It was found during one of our guided school fossil walks. The tooth is 24 mm long from tip to base; it has longitudinal grooves and a near-circular cross section. It may be from a large crocodile similar to Goniopholis which was swimming in the rivers at Yaverland over 122 Million years ago. This is only the crown of the tooth, if the root was still there the tooth would have been much longer. Complete teeth are rare. Its black colouration is due to the fossilization process - the fossil tooth contains a number of black iron compounds. The tooth is amongst the biggest found on this beach.


Strange, but true!
CoproliteOn the 2nd June 2005 this strange object was picked up off the foreshore at Yaverland. It is 16 centimetres long and 6 centimetres thick. Scientifically it is a coprolite, or fossil dinosaur dung (from the Greek Kopros = dung, and lite = mineral, from lithos = stone). It contains the digested remains of a bony meal eaten over 122 million years ago on the Isle of Wight. The lump would have dropped onto the ground as a large steaming heap, from a carnivorous dinosaur. Before it could be disturbed it was covered in mud and fossilized. It remained in the rock for millions of years, until it was found among the pebbles. The biggest lump is 6 centimetres in diameter. You can still see bits of smashed bone amongst the larger lumps which provides evidence that the dinosaur it came from was a carnivore. The coprolite has been given the Museum number IWCMS 2005.85, so it should be available for research for many years.


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